The Southern Annular Mode (SAM) influences phytoplankton communities in the seasonal ice zone of the Southern Ocean

• Format: Dataset
• Language: unknown
• Published: Australian Ocean Data Network
• Subjects: oceans; biota; EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > PROTISTS > PLANKTON > PHYTOPLANKTON; BIOSPHERE > ECOLOGICAL DYNAMICS > COMMUNITY DYNAMICS > COMMUNITY STRUCTURE; OCEANS > OCEAN TEMPERATURE > SEA SURFACE TEMPERATURE; SALINITY/DENSITY > SALINITY; OCEAN CHEMISTRY > NITROGEN; SILICATE; PHOSPHATE; L' ASTROLABE; SOUTHERN ANNULAR MODE; SCANNING ELECTRON MICROSCOPES; SHIPS; LABORATORY; AMD; AMD/AU; CEOS; OCEAN > SOUTHERN OCEAN > SEASONAL ICE ZONE; GEOGRAPHIC REGION > POLAR; CONTINENT > ANTARCTICA; Antarctic; Southern Ocean; The Antarctic; Austral; Astrolabe; Dumont d’Urville; Australian Antarctic Basin; Australian-Antarctic Basin; Antarc*; Antarctica
• Online Access: https://researchdata.edu.au/the-southern-annular-southern-ocean/2819874

Progress Code: completed Statement: One sample does not have NOx, PO4, and SiO4 concentration data Purpose To determine if variation in the SAM (and other environmental variables) is expressed as variation in the community composition of phytoplankton The absolute abundances (cells per ml) of 22 hard-shelled phytoplankon taxa (comprised of species, genera or higher taxonomic groups) estimated from Scanning Electron Microscope survey of 52 samples collected through 11 austral spring-summers (2002/3 to 2012/13) (part of the L' Astrolabe collection) from the seasonal ice zone of the Southern Ocean (between latitude 62 and 64.4 degrees south, and longitude 135.8 and 150 degrees east) also included are environmental covariables for each sample: three constructed SAM indices, SST, Salinity, NOx, PO4, SiO4, and the sampling date, time, and location. Fifty-two surface-water samples were collected from the seasonal ice zone (SIZ) of the Southern Ocean (SO) across 11 consecutive austral spring-summers from 2002/03 to 2012/13. The samples were collected aboard the French re-supply vessel MV L’Astrolabe during resupply voyages between Hobart, Tasmania, and Dumont d’Urville, Antarctica between the 20th October and the 1st March. Most samples were collected from ice-free water, although some were collected south of the receding ice-edge. The sampled area was in the high latitude SO (Figure 1b) in the south-east corner of the Australian Antarctic Basin, spanning 270 km of latitude between 62°S and 64.5°S, and 625km of longitude between 136°E and 148°E. The area lies greater than 100 km north of the Antarctic continental shelf, in waters greater than 3,000 m depth. Samples were obtained from the clean seawater line of the re-supply ship from around 3 m depth. Each sample represented 250 ml of seawater filtered through a 25 mm diameter polycarbonate-membrane filter with 0.8 µm pores (Poretics). The filter was then rinsed with two additions of approximately 2 ml of MilliQ water to remove salt, then air dried and stored in a ...